Mantle convection

Mantle convection is the process by which heat from the Earth's interior causes the movement of the semi-fluid mantle layer, which lies between the Earth's crust and the outer core. This process is a key mechanism in plate tectonics, influencing the movement of tectonic plates on the Earth's surface. Here’s how mantle convection works: 1. **Heat Production**: The Earth's interior generates heat through radioactive decay and residual heat from the planet’s formation.